4.3 Carbon cycle Flashcards
Carbon Dioxide diffusion
From atmosphere into ocean.
Aqueous CO2 binds to H2O to form H2CO3 –> H + HCO3- (Hydrogen Carbonate)
Carbonate ions are used by coral to form the skeleton base (CO32- )
Carbonate ions bond to H to form HCO3-
HCO3- makes the water more acidic.
Carbon cycle features
Pools (producers, consumers, detrits, Fossil fuels)
Flux (Arrows that show direction of Co2)
Methane
CH4
Oxidized to CO2 and H2O in the atmosphere
CH4 + 2O2 –> CO2 + 2H2O
Peat
Forms when organic matter is not fullt decomposed because of acidic and/ or anaerobic conditions in waterlogged soils.
Limestone
Forms from fossilized calcium carbonate in corals.
Is sedimentary rock.
factors impacting Co2 in atmosphere
- Combustion (burning of fossil fuels)
- Deforestation
- Volcanic activity
- Seasons (photosynthesis)
- Forest fires
- Ecosystems developing into climax conditions
when is Co2 released
plants, microbes, animals respire
burning fuels
Carbon fixation
Conversion of inorganic carbon to organic carbon by living things (photosynthesis)
Cell respiration
Conversion of organic carbon back into inorganic carbon
Processes that affect the carbon cycle
- Methane production
- Peat formation
- Coal and oil formation
- Combustion
- Limestone formation
Methanogenesis
Methane is the product from organis matter in anaetobic conditions by methanogenic archaens, some diffuses into the atmosphere
Oxidation of Atmospheric Methane
CH4 + 2O2 -> Co2 + 2H2O
Combustion Sources
Fossil Fuels
- The heat and pressure over time triggers a chemical transformation that results in the compaction of the organic matter
- results are coal, oil and natural gas (non renewable)
- Organism decomposed NOT fossilised
Biomass
- An alternative to relying on fuels produced by geological processes is to manufacture fuels from biological processes
- Living organisms produce hydrocarbons
The ocean
Acts as a large reservior for carbon.
Dissolved Co2 in seawater occurs as 3 inorganic compounds:
- Aqueous Co2
- Bicarbonate (HCO3-)
- Carbonate ions (Co3^2-)
carbon dissolving in seawater process
Co2 binds to H2O
carbonic acid (H2Co3) is formed
It then splits to form H & HCo3-
Increased atmospheric Co2 = increased dissolved Co2 in seawater
= decreased carbonate available for corals